CONTRIBUTION OF VOLCANISM AND TECTONISM TO AXIAL AND FLANK MORPHOLOGYOF THE SOUTHERN EAST PACIFIC RISE, 17-DEGREES-10'-17-DEGREES-40'S, FROM A STUDY OF LAYER 2A GEOMETRY
Sm. Carbotte et al., CONTRIBUTION OF VOLCANISM AND TECTONISM TO AXIAL AND FLANK MORPHOLOGYOF THE SOUTHERN EAST PACIFIC RISE, 17-DEGREES-10'-17-DEGREES-40'S, FROM A STUDY OF LAYER 2A GEOMETRY, J GEO R-SOL, 102(B5), 1997, pp. 10165-10184
Multichannel seismic images from the East Pacific Rise 17 degrees 10'-
17 degrees 40'S are used to study the geometry of seismic layer 2A in
the near-axis region. Wave-equation datuming is applied to stacked com
mon midpoint data to remove the distorting effects of seafloor topogra
phy on the layer 2A event. Processed stacks are compared with seafloor
morphology and tectonic fabric imaged in side-scan sonar data. Assumi
ng layer 2A corresponds with the extrusive crust, these data are used
to study the relationship between volcanism and tectonism in the accum
ulation of the extrusive layer and to assess the contribution of extru
sives to ridge-crest and ridge-flank morphology. We find variations in
axial thickening of layer 2A which imply twofold variation in the wid
th of the extrusive layer accumulation zone, as well as systematic cha
nges in the pattern of accumulation of this layer. On the ridge flanks
the layer 2A horizon mimics abyssal hill relief, consistent with a ho
rst and graben origin for this topography. Short-wavelength variations
in the thickness of layer 2A are superimposed on this relief, which w
e attribute to volcanic modification of tectonic topography at the edg
e of the neovolcanic zone. The integrated off-axis thickness of layer
2A is correlated with ridge cross-sectional area and indicates persist
ent (100,000 years) spatial gradients in extrusive layer thickness. Sy
stematic changes in the cross-axis shape of the ridge, observed over d
istances of 5-10 km, cannot be attributed to the extrusive layer, and
it appears that axial structure beneath the volcanics governs the cros
s-axis morphology of the ridge.